There are 4 main management strategies for reducing the risk from tectonic hazards: monitoring, prediction, protection, planning
Monitoring: volcanoes
All active volcanoes are now monitored using hi-tech scientific equipment including:
Seismometers (seismographs) to detect and record microquakes
Tiltometers to monitor ground deformation as magma rises
Instruments to monitor gas emissions and changes in water chemistry
Monitoring: earthquakes
Earthquakes generally occur without warning. But a network of seismometers monitor and record them
Monitoring: earthquakes
Tsunami monitoring systems in the Pacific and Indian Oceans use floating buoys to detect early tsunami waves following an earthquake. Warnings are then issued using sirens, TV and media alerts
Prediction: volcanoes
Monitoring is now allowing accurate prediction and effective evacuation
Prediction: earthquakes
Accurate predictions are impossible due to a lack of clear warning signs. But historical records can help identify locations at probable risk e.g. Istanbul on the North Anatolian Fault, Turkey
Protection: volcanoes
Earth embankments have been used to successfully divert lava flows (e.g. Mount Etna, Italy). In Japan, weirs and small dams control lahars (mudflows of ash and water)
Protection: earthquakes
Earthquake-resistant engineering of infrastructure and buildings is the best way to reduce risk e.g. seawalls
Planning: volcanoes
Hazard mapping is used to identify areas to control development in at risk areas, and plan evacuation routes (e.g. Mount Merapi, Indonesia)
Planning: earthquakes
Shakemaps (of past impacts) are used to identify lower-risk areas to locate high-value buildings (e.g. hospitals and power stations)